大气波动

  • 网络atmospheric wave
大气波动大气波动
  1. 与用经验正交函数(EOF)对模式气候作分析不同,球谐波谱分析能清晰显示大气波动的物理图像,尤其是全球大气低频波。

    In comparison with model climate analysis by use of the EOF , the spherical harmonics spectral analysis can better reveal the physical pattern of atmospheric waves .

  2. 理想基流中大气波动多折射的数值试验

    Numerical experiments of multi refraction of atmospheric waves on perfect basic flows

  3. 从热带大气波动的频率方程出发,详细分析了过去给出的低频Rossby波的近似频率公式发现其对热带Rossby波的性质有一定程度的歪曲。

    Proceeding from frequency equations of waves in the tropical atmosphere , a detailed analysis of approximate frequency formula of low-frequency Rossby wave given by Matsuno is done in this paper . Results show that the approximate formula misrepresents Rossby wave in the tropical atmosphere in some degree .

  4. 大气波动不稳定与林区降水分布(Ⅱ)

    The instability of atmospheric waves and the precipitation distribution in forest rigions (ⅱ)

  5. 大气波动传播问题的一种无反射数值边界格式

    A Kind of Non-Reflection Numerical Boundary Scheme for the Propagation of Atmosphere Waves

  6. 赤道加热对大气波动的影响

    Heating effects on atmosphere wave in equator

  7. 海气耦合模式中加热函数对大气波动振幅的影响

    The influence of the heating function upon the amplitude of the atmospheric wave in a coupled ocean-atmosphere model

  8. 这扰乱了能够传播数千英里的大气波动,在全球重新分配热量和水分。

    That perturbs atmospheric waves that can travel thousands of miles , redistributing heat and moisture around the globe .

  9. 在一个简化的二层模式中,求解大气波动方程,得到了二维波状起伏地形上扰动流线的分析解。

    In a two-layer model , the wave equation is solved to obtain the resolution analytically of disturbed streamlines caused by a two-dimensional sinusoidal topography .

  10. 在中高纬度地区,大气波动增长标高存在着一定程度的季节变化,冬季的波动增长标高略大,夏季略小。

    The atmospheric wave growth scale height varies seasonally in mid-high latitude . The wave growth scale height is greater in winter and smaller in summer .

  11. 最后,对强迫耗散正压大气波动准共振进行了理论分析,进一步证实了本文的诊断分析和数值试验结果。

    At last , some theory analysis on wave quasi-resonance in forced and dissipative barotropic atmosphere is analysed in theoretics , which further proved the results of diagnosis and numerical experiments is understated .

  12. 由于月球上没有大气,波动无法停止,结果旗子看起来像在随风飘动。

    But on the Moon , where there is no atmosphere , the rippling carried on , making it look like wind .

  13. 本文利用地转动量近似〔1〕并结合行波解的方法,研究了均匀基本气流中的层结大气非线性波动。

    Nonlinear waves in a stratified atmosphere with basic uniform flow are studied by adopting geostrophic momentum approximation ( cf. HosKins , 1975 ) ) and the method of travelling wave solution .

  14. 结果表明:轻质麦秸复合墙体抵抗外界大气温度波动的能力是普通砖墙的8~10倍,具有良好的保温隔热性能;

    The results indicated that the wheat straw-based sandwich wallboard had better property of withstanding the difference of the outdoor environment than the brick wall , which was about 8 ~ 10 times of brick wall .

  15. 而其碳循环速率的微小波动可能造成大气CO2浓度的波动。

    While the small fluctuations of carbon cycle rate may result in a shock to atmospheric carbon dioxide concentration .

  16. 分层热带海洋模式中的Rossby波和Kelvin波&初始混合层深度异常与大气热力强迫激发波动

    Rossby Waves and Kelvin Waves in a Layered Tropical Numerical Ocean Model

  17. 地形对热带大气超长尺度Rossby波动的影响

    The influence of orography on the ultra long Rossby waves in the tropical atmosphere

  18. 在冕洞大气中,由于波动量的淀积而产生的对流能损耗也是重要的,在过渡区底部650km以上,对流能损耗逐渐超过辐射损耗。

    In the transition region at the heights greater than 650 km above the base of the transition region the convection energy losses may gradually exceed the radiation energy losses .

  19. 半地转近似下正压大气中的非线性波动

    The Nonlinear Waves in Barotropic Atmosphere under Semi-geostrophic Approximation

  20. 各树种的蒸腾耗水量的连日变化波动的情况与大气温度和大气相对湿度波动规律一致,随着水分胁迫程度的加剧,树种间与同一树种的差异不再显著。

    Continuous-diurnal variations of water consumption fluctuated with the changes of air temperature and humidity and the difference was not remarkable when the degree of water stress was stronger .

  21. 大气重力波是大气中的基本波动形式之一,在中高层大气动力学过程中起着十分重要的作用。

    Atmospheric gravity wave ( AGW ) is one of the fundamental waves in the atmosphere , which play a very important role in influencing the dynamics in the mesosphere and lower thermosphere ( MLT ) region .

  22. 已有的大气修正方法是基于两个波长激光回波信号受到相同大气波动的基础之上,不适用于这种准同时的工作方式。

    The known atmospheric correction methods based on the same atmospheric effects of two laser signals are not suitable for quasi-simultaneous emissions of two lidar wavelengths .

  23. 为了解决观测和理论研究中的一些问题以及更好地了解热带大气动力学,有必要进一步研究基本气流的变化对大气中赤道Rossby波动的影响。

    In order to tackle the questions arising from the observations and theoretical studies , and to better understand tropical atmospheric dynamics , it is necessary to investigate further the effects of the varying basic states of the atmosphere upon the equatorial trapped nonlinear Rossby waves .

  24. 波动现象是海洋大气边界层的一个重要现象,对发生在海洋大气边界层中的大气波动现象的研究,与海洋、大气科学的其它研究领域及污染治理和环境保护等都有密切关系。

    Waves are one of the very important phenomena occurring in MSBA .